“…(2003) predicted that for near uniaxial magnetite grains of between 30 and 150 nm in size (side length of equivalent cubic volume), magnetostatic interactions in powders are likely to decrease B c and M rs / M s by percentages P h and P m of ∼17% and ∼18%, respectively (Afremov et al., 2018; Fidler & Schrefl, 1996; Muxworthy et al., 2003). We might expect the dipole‐dipole interaction to be proportional to the particles’ decreasing saturation magnetization as the oxidation process occurs (Afremov et al., 2018; Anisimov & Afremov, 2018). Therefore, in order to simulate hysteresis behavior for a powdered sample we might reasonably apply a simple interaction field correction and similarly where B ini and M rs , ini are the initial coercivity and saturation remanence of oxidized magnetite calculated by the average over a lognormal distribution of grain sizes, where B cor and M rs , cor are the counterparts after the interaction field correction, and B mag and M rs , mag are the corresponding equivalents of stoichiometric magnetite.…”